Orbicella faveolata in St. Croix, USVI
The NOAA Atlantic Oceanographic and Meteorological Laboratory (AOML) conducts the long-term National Coral Reef Monitoring Program (NCRMP) to track the status and trends of coral reef ecosystems of the U.S. Atlantic and Caribbean coral reef jurisdictions. This summary brief provides an overview of the most recent survey efforts to Puerto Rico.
| Location | 1m | 5m | 15m | 25m | Total |
|---|---|---|---|---|---|
| Arecibo | 105,139 | 557,457 | 298,970 | 568,609 | 1,530,175 |
| Culebra | 238,140 | 211,204 | 331,928 | 306,518 | 1,087,790 |
| Jobos Bay | 605,123 | 316,687 | 622,946 | 512,922 | 2,057,678 |
| La Parguera | 622,965 | 513,059 | 362,198 | 404,737 | 1,902,959 |
| Rincon | 453,283 | 286,086 | 270,786 | 384,289 | 1,394,444 |
| Fajardo | NA | 479,577 | 178,362 | 575,034 | 1,232,973 |
## [1] "pH = 205 observatons"
## [1] "Current = 205 observatons"
## [1] "Light = 202 observatons"
Figure 1: Study sites and depths in Puerto Rico.
The temperatures that marine organisms experience are a function of local oceanographic conditions and vary with depth. To monitor subsurface temperature, six transects were established around the island. Each transect consists of STRs at four depths (1, 5, 15, 25m; Fig.2). Two years of temperature measurements were retrieved and processed from the 24 sites. Temperature was measured using SeaBird Electronics Subsurface Temperature Recorders (STR)s that collected data at 5-minute intervals. The COVID - 19 pandemic delayed collection in 2020 and local contractors were hired to swap the instruments as travel was not allowed. Some gaps exist in the data as not all instruments survived the extended deployment time. The entire record from 2017 to 2023 is shown to aid with comparison.
Figure 2: Temperature conditions at six locations in Puerto Rico (Rincon, Arecibo, Jobos Bay, La Parguera, Culebra, Fajardo) representing a depth gradient (1m, 5m, 15m and 25m). Data were collected from XX 2017 to May 2023 However, the COVID 19 pandemic caused a significant delay in collection of these instruments. Contractors were hired to complete the work in 2021 as travel was not allowed. Some instruments survived the entire deployment but others have not.
Mean temperature values were similar among the locations and depths. The lowest temperatures generally occurred in February (mean: 26.5\(^\circ\)C, min: 24.7\(^\circ\)C, max: 28.5\(^\circ\)C) and the highest temperatures in September (mean: 29.4\(^\circ\)C, min: 25.4\(^\circ\)C, max: 32.2\(^\circ\)C). explain more gaps and issues here?
Seawater carbonate chemistry can fluctuate diurnally, due to biological forcing processes such as photosynthesis andrespiration, as well as calcification and dissolution. Tocharacterize this, discrete water samples (Fig. 3) were collected at three-hour intervals (n=15) using SubsurfaceAutomatic Samplers (SAS, www.coral.noaa.gov/accrete/sas).
These samples will be analyzed for Total Alkalinity (TA), Dissolved Inorganic Carbon (DIC), and SpectrophotometricpH (SpecpH), which will be used to calculate pCO2 and aragonite saturation state (ΩAragonite). A suite of instrumentswas deployed for a 72-hour period at the East Bank 20m site. A SeaFET was used to log pH, an EcoPAR measured Photosynthetically Active Radiation (PAR), and a Lowell Tiltmeter measured current speed and direction. Each collected measurements at 15-minute intervals (Fig. 2).
Figure 3: Data from La Parguera diurnal suite monitoring from May 21st to May 23rd. Top panel: pH and temperature fromSeaFET. Bottom panel: Photosynthetically Available Radiation (PAR) and current speed from EcoPAR and Tiltmeter. Shading denotes nighttime throughout sequence of the plot. Instruments measured parameters every 15 minutes.
Figure 4: Submered Automated Samplers (SAS) deployed to collect water samples every 3 hours
Figure 5: Carbonate budgets XX in 2015, 2017 and 2023 and the processes contributing to calcification and bioerosion. Carbonate budgets were stable among the years surveyed, with stable coral production and minimum variatons in bioerosion.
The transect results showed positive carbonate budgets in 2015, 2017 and 2023, which implies that this site supported reef accretion over the past eight years.
Figure 6: CAU and BMU pair before retreval after being deployed for 3 years. CAUs are 2 parallel PVC plates to quantify settled accretors. BMU is mounted coral skeleton installed at the base of the metal stake and has been encrusted.
AOML’s climate monitoring is a key part of the National Coral Reef Monitoring Program of NOAA’s Coral Reef Conservation Program (CRCP), providing integrated, consistent, and comparable data across U.S. Managed coral reef ecosystems. CRCP monitoring efforts aim to:
Atlantic Climate team lead: nicole.besemer@noaa.gov
Principal Investigator: ian.enochs@noaa.gov
NCRMP Coordinator: erica.towle@noaa.gov
Coral Reef Conservation Program: http://coralreef.noaa.gov
NCRMP climate monitoring: https://www.coris.noaa.gov/monitoring/climate.html
NOAA Atlantic Oceanographic and Meteorological Laboratory: http://www.aoml.noaa.gov/
These efforts were jointly funded by NOAA’s CRCP and OAP. We would like to sincerely thank the National Park Service as well as Caribbean Sea Adventures for supporting our field efforts and assisting monitoring surveys
Puerto Rico, 2023 Field team
AOMLs NCRMP Atlantic and Caribbean Climate Team: I. Enochs, N. Besemer, G. Kolodziej, A.Boyd, M. Jankulak, A. Palacio-Castro, A. Webb, B. Chomitz